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Estimation of the spatial distribution of soil erosion in the hilly area of Sichuan, China

机译:四川四川丘陵区土壤侵蚀空间分布的估算

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The hilly area of Sichuan (China) has suffered from soil erosion as a result of the intensive agriculture and steep topography. Many different methods have been used for the estimation of soil erosion and no clear consensus about erosion rates and subsequent sediment delivery ratios (SDR) has been reached. In this study, the Universal Soil Loss Equation (USLE) with different parameter estimation methods was applied to two river basins (i.e. Weichenghe (WCH) and Lizixi (LZX)) with the help of GIS techniques. The results were compared with those of previous studies based on remote sensing, erosion plots or the ~(137)Cs technique. The main results can be summarized as: (1) different rainfall erosivity estimation methods generate vastly different results; (2) using two-dimensional slope length produces higher soil erosion rate estimates and lower SDRs than the conventional approach in USLE; (3) the average annual soil erosion rates for WCH and LZX were estimated at 706 t km~(-2) year~(-1) and 3040 t km~(-2) year~(-1), respectively, and the corresponding sediment delivery ratios at 0.27 and 0.38; and (4) the high erosion rates reflect the high altitude and intensive agricultural land use.
机译:川中丘陵区(中国)已经从土壤侵蚀遭受集约农业和地形陡峭的结果。许多不同的方法已用于土壤侵蚀的估计和对侵蚀速率和随后的泥沙输移比(SDR)没有明确的共识已经达成。在这项研究中,通用土壤流失方程(USLE)使用不同的参数估计方法被应用于两个流域(即Weichenghe(WCH)和Lizixi(LZX))与GIS技术的帮助。将结果与基于遥感,侵蚀曲线或〜(137)Cs的技术的那些以前的研究的进行了比较。主要结果可归纳为:(1)不同的降雨侵蚀力估算方法产生截然不同的结果;使用二维斜率长度(2)产生较高的土壤侵蚀速率估计和比USLE传统方法的SDR更低; (3)年平均土壤侵蚀对WCH和LZX率估计为706吨公里〜(-2)年〜(-1)和3040吨公里〜(-2)年〜(-1),分别与在0.27和0.38相对应的沉积物输送比率; (4)高耐冲蚀率反映了高海拔和集约化农业用地。

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